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沙特阿拉伯东部地区艾哈萨绿洲地下水化学及其对土壤性质的预测影响。

Chemistry of groundwater of Al-Ahsa Oasis eastern region Saudi Arabia and its predictive effects on soil properties.

作者信息

Al-Zarah Abdullah I

机构信息

National Center for Water Research (NCWR), King Abdulaziz City for Science and Technology (KACST), P.O. Box 6086, Riyadh 11442, Saudi Arabia.

出版信息

Pak J Biol Sci. 2008 Feb 1;11(3):332-41. doi: 10.3923/pjbs.2008.332.341.

Abstract

Saudi Arabia is an arid and the largest country in the middle east with a total land area of 2.253 x 10(6) km2. Recent urban and rural expansion has shown manifold increases in water use in various sectors. Water resources are limited and non-renewable coupled with unpredicted scanty rainfall. In order to meet the rising water needs, evaluation of water quality is important for allocation to various uses. A total of 101 well water samples were collected from Al-Ahsa Oasis. Water samples were analyzed for total salt concentration, pH, Ca, Mg, Na, K, HCO3, Cl, SO4, NO3, F and B contents. Soil Salinity Development (SSD), adjusted sodium adsorption ratio (adj.SAR), adjusted sodium adsorption ratio (adj. R(Na)) and Exchangeable Sodium Percentage (ESP) were calculated. The EC of groundwater ranged between 1.23 and 5.05 dS m(-1). Sodium was the most abundant cation followed by Ca, Mg and K in descending order. Chloride was the most abundant anion followed by SO4 and HCO3 in groundwater of Al-Ahsa Oasis. A significant correlation was found between Na and Cl (R2 = 0.936). Thermodynamics calculation revealed that an appreciable amount of Ca and Mg is associated with Cl and SO4 ions. The SAR and ESP values are within the permissible limits according to Ayers and Westcot, 1985. The NO3 concentration is within safe limits for drinking purpose according to WHO (1998) standards. The Saturation Indices (SI) indicated that groundwater is under-saturated (negative SI) with respect to certain minerals (for example: calcite, dolomite, gypsum, anhydrite, halite, pyrite, fluorite and aragonite) and oversaturated (positive SI) with respect to some other minerals (For example: Goethite, Siderite and hematite). The negative saturation index (SI) reveals that most of minerals are in un-saturated state and will dissolve more Ca and Mg into the soil solution after irrigation. A good relationship exists between Cl and other ions (Na, Ca and Mg) as well as between SO4 and Ca and Mg ion of groundwater. The salinity and sodicity hazards of groundwater of Al-Ahsa Oasis were classified as C3S1 and C4S2 i.e., high salinity with medium sodicity problems. The predicted soil salinity suggested application of 15-20% leaching requirements to keep soil salinity within permissible limits. Cultivation of slight to moderate salt and sodium tolerant crops is recommended for optimal agricultural production and efficient water use.

摘要

沙特阿拉伯是中东地区一个干旱且面积最大的国家,陆地总面积为2.253×10⁶平方千米。近期城乡的扩张使得各部门用水量呈多倍增长。水资源有限且不可再生,同时降雨稀少且难以预测。为了满足不断增长的用水需求,评估水质对于分配各种用途至关重要。从哈萨绿洲共采集了101份井水样本。对水样分析了总盐浓度、pH值、钙、镁、钠、钾、碳酸氢根、氯、硫酸根、硝酸根、氟和硼的含量。计算了土壤盐分发展(SSD)、调整后的钠吸附比(adj.SAR)、调整后的钠吸附比(adj.R(Na))和交换性钠百分比(ESP)。地下水的电导率范围在1.23至5.05 dS m⁻¹之间。钠是最丰富的阳离子,其次是钙、镁和钾,顺序依次递减。在哈萨绿洲的地下水中,氯是最丰富的阴离子,其次是硫酸根和碳酸氢根。钠与氯之间存在显著相关性(R² = 0.936)。热力学计算表明,相当数量的钙和镁与氯和硫酸根离子相关联。根据艾尔斯和韦斯科特1985年的标准,SAR和ESP值在允许范围内。根据世界卫生组织(1998年)标准,硝酸根浓度在饮用安全限度内。饱和指数(SI)表明,地下水相对于某些矿物质(例如:方解石、白云石、石膏、硬石膏、石盐、黄铁矿、萤石和文石)处于不饱和状态(负SI),而相对于其他一些矿物质(例如:针铁矿、菱铁矿和赤铁矿)处于过饱和状态(正SI)。负饱和指数(SI)表明大多数矿物质处于不饱和状态,灌溉后会有更多的钙和镁溶解到土壤溶液中。地下水中氯与其他离子(钠、钙和镁)之间以及硫酸根与钙和镁离子之间存在良好的关系。哈萨绿洲地下水的盐分和碱化危害被分类为C3S1和C4S2,即高盐分且伴有中等碱化问题。预测的土壤盐分表明需要施加15 - 20%的淋洗需求,以将土壤盐分保持在允许范围内。建议种植轻度至中度耐盐和耐钠作物,以实现最佳农业生产和高效用水。

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